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Analysis of the spatial and temporal sensitivities of key parameters in the SWAN model: An example using Chan-hom typhoon waves

机译:SWAN模型中关键参数的时空敏感性分析:使用Chan-hom台风波的示例

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In this work, the spatial and temporal sensitivities of the significant wave height (SWH) to ten key parameters in the SWAN model under typhoon conditions are assessed through comprehensive observations at four buoy stations along the eastern coast of China. Experiments were conducted using wind forcing based on Typhoon Chan-hom, which made landfall at Zhujiajian island in 2015. Assessments included wind input and whitecapping, bottom friction, depth-induced wave breaking, and nonlinear quadruplet wave interactions parameterizations. The results show that in shallow water whose depth is less than the threshold depth, depth-induced wave breaking dominates the SWH, and the SWH is most sensitive to the parameter gamma (the ratio of maximum individual wave height to depth) of depth-induced wave breaking. However, beyond a certain threshold depth, the sensitivity of the SWH to depth-induced wave breaking begins to reduce. This threshold depth depends on sea states and ranges from 5 m to 30 m. In deep water, where the water depth is more than the threshold depth, SWH is primarily influenced by wind input and whitecapping. In general, the sensitivity is greater in coastal areas than in the open ocean. With regard to sea state, the higher the sea state, the deeper the threshold depth. The four different numerical procedures of four-wave interactions (so-called quadruplets) mainly affect the distribution of wave energy, not the SWH. In addition, the SWH is most sensitive to the drag coefficient, and bigger wave implies greater sensitivity. The study of spatial and temporal sensitivities of key parameters is of great significance for further application of the SWAN model and wave simulations, especially typhoon wave simulations.
机译:在这项工作中,通过对中国东部沿海四个浮标站的综合观测,评估了台风条件下有效波高(SWH)对SWAN模型中十个关键参数的时空敏感性。实验是使用基于台风“ Chan-hom”的强风进行的,该风于2015年在朱家尖岛登陆。评估包括风输入和白峰覆盖,底部摩擦,深度诱发的波浪破碎以及非线性四重波相互作用参数化。结果表明,在深度小于阈值深度的浅水中,深度感应波的破坏主要作用于SWH,而SWH对深度感应参数γ(最大个体波高与深度之比)最敏感。破浪。但是,超过一定的阈值深度,SWH对深度引起的波破坏的敏感性开始降低。该阈值深度取决于海况,范围为5 m至30 m。在深水中,水深大于阈值深度,SWH主要受风输入和白顶影响。通常,沿海地区的敏感性要比公海中的敏感性高。关于海况,海况越高,阈值深度越深。四波相互作用的四种不同数值过程(所谓的四联体)主要影响波能的分布,而不影响SWH。此外,SWH对阻力系数最敏感,并且更大的波浪意味着更大的灵敏度。关键参数的时空敏感性研究对SWAN模型和海浪模拟,尤其是台风海浪模拟的进一步应用具有重要意义。

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